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排序方式: 共有1422条查询结果,搜索用时 15 毫秒
1.
I.CORRELATIONBETWEENL0ESSSECTI0NAND0XYGENIS0TOPESTAGESIntheYuanloessarea,manyscientiststhinkthatthesedimentsarecontinuousandtheclimaticrecordsareperfect.Thisdoesnotappeartobeaccurate.Sedimentationwasdiscontinuousinmanysections.Forexample,manyscientistsarguethatS2corresp0ndstooxygenisot0peStage7(Liu,l985,KuklaandAn,l989;Dingetal.,l990).lnfact,S2includesthreelayersfS2SSl,S2LLlandS2SS2.Dingetal.(l990)reportedthatthereisathickunitofloessbetweenS2SSlandS2SS2intheBaicao… 相似文献
2.
A palaeocommunity of large Conichnus conicus, a conical, cone-in-cone shaped burrow, created by sea anemones, occurs in medium-grained, crossbedded, well-sorted sandstone in the middle part of the Cretaceous Guneri Member of the Bhuj Formation in India. The trace fossil Conichnus is considered to be a common element of the Skolithos ichnofacies and is interpreted to reflect equilibrium movement in response to substrate aggradation. In the present study, three different varieties of Conichnus conicus are distinguished based on morphology and internal fabric. Community dynamics and burrowing behavior are revealed by inter-burrow relationships, burrow initiation levels and sedimentology. Three types of behavior are envisaged: retrusive equilibrium, protrusive equilibrium response, and escape behavior. Palaeocommunity dynamics show that the tracemakers consisted of only adult organisms that initiated burrows during neap tides and are adapted to feed effectively during weak flow conditions. The occurrence of Conichnus palaeocommunity in the Guneri Member indicates the tidal conditions in a fully marine setting. Results presented herein may aid in the understanding of palaeocommunity dynamics in other shallow marine sequences. 相似文献
3.
山西永济白草坪组具刺疑源类的发现及其地质意义 总被引:13,自引:0,他引:13
该文着重报道了山西永济白草坪组(一般认为系中元古界上部相当于蓟县系的层位),以具刺疑源类为主的微化石群,计有4类6属15种,其中包括1新属,4新种,1新组合,1亲近种,2未定种,新属是具细网状纹饰的复杂具刺疑源类Shuiyousphaeridium Yan gen.nov.,4新种是Shuiyousphaeridium membraniferum Yan sp.nov.,Dictyosphaera incrassate Yan sp.nov.,Foliomorpha stipuliferaYan sp.nov.,Manicosiphoninema shuiyouense Yan sp.nov.。本微化石群以球形疑源类为主体,以具刺疑源类的大量发育为特征,并伴生有推测是绿藻和褐藻的化石,其组合面貌与蓟县上前寒武系各组皆有明显区别,具有更高的进化程度,从生物地层标志推测白草坪组所在的汝阳群应归入震旦系。白草坪组具刺疑源类可能是横裂甲藻的原始分子,它在地层对比和藻类进化方面皆具有重要意义。 相似文献
4.
该文研究的轮藻化石采自尼泊尔中西部阿龙科拉地区的比奈科拉组下段。轮藻化石有Nitellopsis (Tectochara)globula(Madler)Grambast et Soulie-Marsche,Chara molassica Straub,C.gigantofusiformis(Yang),Rantzieniella binaiensis sp.nov.,Gyrogona arungensis sp.nov.和Lychnotharnnuspseudoodea(Berger)Soulie-Marsche等,此轮藻化石植物群属新第三纪,可能为中新世晚期。克里雅群轮藻的研究将增添南亚新第三纪地质生态研究的内容。 相似文献
5.
Révision d'?Orthis? berthoisiRouault, 1849Orthida (Brachiopoda) de l'Ordovicien du Massif Armoricain
Michel Melou 《Geobios》1985,18(5):595-607
Since it is impossible to state about any genericassignment for Orthis berthoisiRouault, 1849the species name is herein restricted to original specimens figured by the author. The study of the Brachiopods from the St-Germain-sur-Ille Formation allows to confirm the first determination by De Tromelin &Lebesconte (1875)and to establish their conspecificity with Orthis berthoisi var. erratica described in 1869 by Davidson from the Budleigh-Salterton pebbles. The successive assignment of the species erratica to the genus Svobodaina(Cocks, 1978) then to Corineorthis(Cocks & Lockley, 1981) is discussed. The attribution to the genus DrabovinellaHavlicek, 1951appears most likely. 相似文献
6.
The vegetation succession on the dunes near Oostvoorne, The Netherlands has been followed by means of a novel combination of repeated large-scale vegetation mapping and air photograph interpretation. Vegetation units have been discerned on the formation level because these could be distinguished fairly easily on the photographs and because the rates of change are appropriate to the time interval chosen. Nineteen formations were distinguished. Five 1:6250 maps were constructed, reflecting the formation pattern in 1934, 1943, 1959, 1972 and 1980. An overlay with 2736 grid points at 25 m field distance was used to quantify changes in the formation pattern.The results suggest a pronounced multiple pathway succession with nevertheless three principal trajectories of succession from pioneer to woodland vegetation. The outer dunes, which have originated since 1910, are distinct in successional characteristics from the inner dunes, which already existed but were released from heavy grazing pressure in 1910. The rate of change in the outer dunes was high in the beginning and is slowly decreasing eversince. In the inner dunes it went the other way around. Through visual extrapolation the likely formation patterns in 1910 and in 2000 were estimated.Transition frequencies proved highly variable for most formations. Moreover, strong spatial dependence was found. Limitations in the use of Markov models in cases of long-term succession in heterogeneous environments are discussed.Nomenclature follows the same sources as in van der Maarel et al. (1984).Field work carried out 1980–1981 when the authors were at the Division of Geobotany, University of Nijmegen. We thank Jos Rijntjes, Nijmegen, for his cooperation in the field. Vegetation maps were prepared and calculations performed at Uppsala. We thank the Foundation Het Zuid-Hollands Landschap, Rotterdam, for providing facilities and a grant for fieldwork as well as additional means to reproduce the vegetation maps. Two reviewers gave useful comments. 相似文献
7.
皖南、赣北奥陶纪笔石立体标本形成环境的初步研究* 总被引:1,自引:0,他引:1
皖南、赣东北和赣西北地区奥陶纪笔石地层发育良好,笔石化石丰富。宁国组和胡乐组均为笔石相地层,但笔石的保存特点并不相同。立体保存的黄铁矿化笔石标本主要见于宁国组,而胡乐组的笔石几乎均为薄膜标本。在比较宁国组和胡乐组在岩性、颜色、化石、矿物和元素等方面的特点后发现,两者有较明显的差异。这表明宁国组和胡乐组形成时的环境是不同的,前者为弱还原环境,后者为较强的还原环境,而在研究区内影响笔石体立体保存的主要因素为还原环境和较高的铁含量。在还原环境下,铁可呈Fe~(2+)存在,笔石体内含有硫,死亡后经降解作用可生成H_2S;H_2S和Fe~(2+)结合可使笔石体黄铁矿化,从而使笔石体硬化而呈立体保存下来。宁国组的铁含量明显高于胡乐组,这似可以解释宁国组产有较多笔石立体标本的原因。 相似文献
8.
黑龙江绥滨地区晚侏罗世东荣组的沟鞭藻类 总被引:12,自引:0,他引:12
本文对黑龙江绥滨86-11孔的沟鞭藻类进行了初步研究,共描述化石10属16种(包括2新种,6未定种);其中不少是在我国首次描述的。这些化石分成两个组合,其优势分子分别为Gonyaulacysta jurassica和Amphorula delicata。根据组合内各分子的时代分布,两化石组合的时代分别为Late Oxfordian—Early Kimmeridgian和Portlandian期,并对其产出层位东荣组的时代作了讨论,认为属于晚侏罗世。 相似文献
9.
G. Menestrina C. Pederzolli M. Dalla Serra M. Bregante F. Gambale 《The Journal of membrane biology》1996,149(2):113-121
Escherichia coli hemolysin is known to cause hemolysis of red blood cells by forming hydrophilic pores in their cell membrane. Hemolysin-induced
pores have been directly visualized in model systems such as planar lipid membranes and unilamellar vesicles. However this
hemolysin, like all the members of a related family of toxins called Repeat Toxins, is a potent leukotoxin. To investigate
whether the formation of channels is involved also in its leukotoxic activity, we used patch-clamped human macrophages as
targets. Indeed, when exposed to the hemolysin, these cells developed additional pores into their membrane. Such exogenous
pores had properties very different from the endogenous channels already present in the cell membrane (primarily K+ channels), but very similar to the pores formed by the toxin in purely lipidic model membranes. Observed properties were:
large single channel conductance, cation over anion selectivity but weak discrimination among different cations, quasilinear
current-voltage characteristic and the existence of a flickering pre-open state of small conductance. The selectivity properties
of the toxin channels appearing in phospholipid vesicles were also investigated, using a specially adapted polarization/depolarization
assay, and were found to be completely consistent with that of the current fluctuations observed in excised macrophage patches.
Received: 14 August 1995/Revised: 2 October 1995 相似文献
10.
PETER D. KRUSE 《Lethaia: An International Journal of Palaeontology and Stratigraphy》1996,29(3):213-217
A single specimen of the early Middle Cambrian (Ordian) orthothecimorph hyolith Gudugu-wan hardmani with preserved gut filling has been discovered in the Montejinni Limestone, Wiso Basin, northern Australia. This represents only the eighth such occurrence worldwide. The specimen is unique among orthothecimorphs in retaining the gut filling in combination with the external mould of the operculum and invites revision of the accepted soft-part recon struction in this group, whereby the opercular lateral processes are now recognized to be ventral. Thus orthothecimorph conchs, if horizontal in life, would have been oriented ventral side down, while hyolithomorphs adopted the reverse orientation: horizontal, ventral side up. 相似文献